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      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="normal" font="default" size="100%">Krien, Y.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Karpytchev, M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Ballu, V.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Becker, M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Grall, C.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Goodbred, S.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Calmant, Stéphane</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Shum, C. K.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Khan, Z.</style>
          </author>
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      <titles>
        <title>Present-day subsidence in the Ganges-Brahmaputra-Meghna delta : eastern amplification of the Holocene sediment loading contribution</title>
        <secondary-title>Geophysical Research Letters</secondary-title>
      </titles>
      <pages>10764-10772</pages>
      <keywords>
        <keyword>land subsidence</keyword>
        <keyword>sediment loading</keyword>
        <keyword>relative sea level rise</keyword>
        <keyword>Ganges-Brahmaputra-Meghna Delta</keyword>
        <keyword>INDE</keyword>
        <keyword>BANGLADESH</keyword>
        <keyword>GANGE BRAHMAPOUTRE MEGHNA DELTA</keyword>
        <keyword>BENGALE GOLFE</keyword>
      </keywords>
      <dates>
        <year>2019</year>
      </dates>
      <call-num>fdi:010077054</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Geophysical Research Letters</full-title>
      </periodical>
      <isbn>0094-8276</isbn>
      <accession-num>ISI:000489485000001</accession-num>
      <number>9</number>
      <electronic-resource-num>10.1029/2019gl083601</electronic-resource-num>
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          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers20-11/010077054.pdf</url>
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      <volume>46</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>The subsidence of the Ganges-Brahmaputra-Meghna Delta (GBMD) drastically increases the adverse impacts of coastal flooding and exacerbates the vulnerability of populations from ongoing rapid sea level rise. We focus here on estimating the present-day subsidence rates induced by the loading of sediments continuously deposited within the GBMD over the past 11,000 years. By constructing a realistic GBMD 3-D numerical model with laterally variable mantle and lithospheric structure, we demonstrate for the first time that the presence of the strong Indian Craton and the weakened Indo-Burma margin results in significant amplification of subsidence driven by sediment loading in the eastern part of the delta, where the population density is the highest (&gt;1,000 habitants per km(2)). Although uncertainties remain regarding the amplitude of subsidence, the rate estimates (2-3 mm/year) are found to be comparable to the present-day global mean sea level rise.</abstract>
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      <custom7>Bangladesh / Chine</custom7>
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